GWSC-VMR, a GIS supported conceptual distributed hydrological model for cold and arid regions

T. Fang, Guizuo Wang, L. Ren
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Abstract

Our research focuses on the study of the particular hydrological process in cold and arid regions. Our aims are to develop a Geographical Information System (GIS) supported conceptual model that could be applied to simulate a drainage basin's hydrological process in cold and arid regions and to verify it through a case study. We built a model named the Vertically-Mixed Runoff Model with Grid-based Water Storage Capacity (GWSC-VMR for short). GWSC-VMR includes two parts, i.e. the spatial distributed model of water storage capacity and the vertically-mixed runoff module. First, drainage basin land cover map and typical vegetation rooting depth were acquired by interpreting remote sensing images or accessing land cover database. Second, through the processing of DEM data, we decided water flow direction, catchment area, basin boundary, and the slope of grided basin. Third, we determined the spatial distribution of water storage capacity based on the vegetation rooting depth. Because vegetation root system is a complicated system which is affected by the depth of active soil layer, and the depth of active soil layer is related to the slope, we put forward a series of concepts—upper critical slope gradient, lower critical slope gradient and critical soil layer depth to describe the grid tension water storage capacity and the grid free water storage capacity. Lastly, we integrated the vertically-mixed runoff mechanism and the spatial distribution of drainage basin water storage capacity to develop the GWSC-VMR, which could be applied to simulate drainage basin hydrologic processes, such as snow melt, canopy interception, evapotranspiration, and flow concentration.
GWSC-VMR,一个GIS支持的寒旱区概念分布式水文模型
我们的研究重点是研究寒冷和干旱地区特殊的水文过程。我们的目标是开发一个地理信息系统(GIS)支持的概念模型,该模型可用于模拟寒冷和干旱地区流域的水文过程,并通过案例研究对其进行验证。本文建立了基于网格的垂直混合径流模型(GWSC-VMR)。GWSC-VMR包括蓄水量空间分布模型和垂直混合径流模块两部分。首先,通过遥感影像解译或访问土地覆盖数据库获取流域土地覆盖图和典型植被生根深度;其次,通过对DEM数据的处理,确定水流方向、集水区面积、流域边界和栅格流域坡度;第三,基于植被生根深度确定了库容的空间分布。由于植被根系是一个受活性土层深度影响的复杂系统,而活性土层深度又与坡度有关,因此提出了上临界坡度、下临界坡度和临界土层深度等一系列概念来描述格栅张力蓄水量和格栅自由蓄水量。最后,将垂直混合径流机制与流域储水量空间分布相结合,开发了GWSC-VMR,可用于模拟流域融雪、冠层截流、蒸散发和水流浓度等水文过程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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